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(Figure 5) Stratigraphic ranges of selected planktonic foraminifers at ODP Ho...
Species abundance: T = trace (one specimen), R = rare (<3%), F = few (3-15%), C = common (16-30%), A = abundant (>30%), P = present, samples with too few planktonic... -
Late Miocene warming in the tropic based on planktonic foraminiferal assemblages
Planktonic foraminifera data was collected using a surface sampling in Kali Pasir River-Banyumas Basin, Central Java, Indonesia (1,300 m measured section of sampling area). The... -
(Appendix A) Distribution of planktonic foraminifera at DSDP Hole 72-516
Numbers have been rounded to the nearest percent. -
(Appendix A5) Planktonic foraminifera of ODP Hole 172-1063A
This dataset has no description
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(Appendix A4) Planktonic foraminifera of ODP Hole 172-1062B
This dataset has no description
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(Appendix A3) Planktonic foraminifera of ODP Hole 166-1006A
This dataset has no description
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(Appendix A2) Planktonic foraminifera of ODP Hole 159-958A
This dataset has no description
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(Appendix A1) Planktonic foraminifera of ODP Hole 157-951A
This dataset has no description
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(Table 16) Distribution of planktonic foraminifers in ODP Hole 108-667A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 15) Distribution of planktonic foraminifers in ODP Hole 108-666A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
Abundance of planktonic foraminifera from IODP Hole 339-U1386C
The base of the Faro contouritic drift (IODP Site U1386) on the northern margin of the Gulf of Cádiz (Algarve margin) is characterized by two sequences of frequent gravity... -
Distribution of planktonic foraminifera in DSDP Hole 31-296 (Table III)
Late Neogene planktonic foraminiferal biostratigraphy of DSDP Site 296, Leg 31, reveals this site as an ideal reference section for correlation of Blow's low-latitude zonation...
